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dc.contributor.authorFernández Puga, María Carmen
dc.contributor.authorVázquez Garrido, Juan Tomás
dc.contributor.authorHernández Molina, F. Javier
dc.contributor.authorSomoza, L.
dc.date.accessioned2015-02-17T10:59:56Z
dc.date.available2015-02-17T10:59:56Z
dc.date.issued1999
dc.identifier.urihttp://hdl.handle.net/10272/9941
dc.description.abstractThe north-western continental margin of the Alboran Sea is characterised by the development of some submarine channels systems during the Pliocene-Quaternary times. One of these systems, the Paleocanyon of Estepona, has been studied by the analysis of multichannel seismic reflection profiles, in the context of the stratigraphical margin building and the tectonic control. Six stratigraphical units of this age have been defined, the lower three units (Lower to Middle Pliocene) are separated from the three upper (Upper Pliocene to Quaternary) by the main erosive discontinuity D3 of the margin, which is correlated with an eustatic fall of third order, of Upper Pliocene age (around 3 M.a.J. The evolution of this paleochannel has been related to eustatic cycles. The paleochannel position is related with deformation in the Miocene units, but fault control is not evidenceden_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherPaleochannelsen_US
dc.subject.otherContinental marginen_US
dc.subject.otherPlioceneen_US
dc.subject.otherQuaternaryen_US
dc.subject.otherAlboran Seaen_US
dc.titleEl Paleocañón de Estepona como un rasgo morfosedimentario Plioceno-Cuaternario del margen septentrional del Mar de Alboránen_US
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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